We present evidence that transparent exopolymer particles (TEP) accumulate in the northern Adriatic Sea as a result of the intrusion of oligotrophic high-salinity water (OHSW) from the south during summer. Samples were collected in June and July of 2007 in haloclines, and in the layers above and below them, at 2 stations in the region of the highest influx of OHSW. In June, we observed that concentrations of TEP in the upper part of the water column were 10 times higher at the eastern station as compared to the western station. This coincided with an intrusion of OHSW at the eastern station while the western station remained unaffected. In July, 2 stronger events involving OHSW encompassed both stations, leading to significant accumulations of TEP in the haloclines and in the layers above. Furthermore, during the period of maximal TEP accumulation, we noted pronounced increases in the abundance of diatoms and in bacterial numbers. These increases coincided with low cell-specific production of bacterial biomass, and a low abundance of actively respiring (CTC+) bacteria. In contrast, during the period of lower TEP concentration in the halocline, we observed an increase in the abundance of CTC+ bacteria, and in cell-specific β-glucosidase activity, probably indicating enhanced degradation of TEP in this layer.KEY WORDS: Oligotrophic high-salinity waters · Transparent exopolymer particles · TEP · Bacterioplankton · Production · Activity · Halocline · Northern Adriatic Sea
Resale or republication not permitted without written consent of the publisherAquat Microb Ecol 63: [69][70][71][72][73][74] 2011 teria, actively respiring (CTC+) bacteria, bacterial production (measured by incorporation of 3 H-leucine and 3 H-thymidine) and β-glucosidase activity.
MATERIALS AND METHODSSampling and basic parameters. During monitoring cruises aboard the 'Vila Velebita' research vessel, from May 10 to July 26, 2007, salinity was determined by CTD profiler (Seabird) at 14 stations of the Rovinj-River Po transect in the northern Adriatic Sea (Fig. 1). Samples for TEP determination were taken with Niskin samplers at the surface, and at depths of 5, 10, 20 and 31 m at Stn SJ103. During additional cruises, conducted on June 11 (Stn SJ105) and July 16 (Stns SJ103 and SJ105, Fig. 1), seawater was collected by SCUBA divers with Niskin samplers placed horizontally at 4 depths. Except for surface samples, the choice of sampling points was made according to salinity data obtained by the CTD profiler to correspond to the halocline layer and the water layers above and below it. For determination of chl a concentration, seawater was filtered through GF/C filters, extracted in acetone (90% v/v) and determined fluorometrically (Strickland & Parsons 1972).
Microphytoplankton and TEP.For microphytoplankton counts, 200 ml samples were preserved with Lugol's solution and stored at 4°C. Microphytoplankton (i.e. cells or colonies > 20 µm) were identified and counted by an inverted microscope (Carl Zeiss) using the settling technique (Ut...